<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">OALibJ</journal-id><journal-title-group><journal-title>Open Access Library Journal</journal-title></journal-title-group><issn pub-type="epub">2333-9705</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/oalib.1102203</article-id><article-id pub-id-type="publisher-id">OALibJ-69006</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Biomedical&amp;Life Sciences</subject><subject> Business&amp;Economics</subject><subject> Chemistry&amp;Materials Science</subject><subject> Computer Science&amp;Communications</subject><subject> Earth&amp;Environmental Sciences</subject><subject> Engineering</subject><subject> Medicine&amp;Healthcare</subject><subject> Physics&amp;Mathematics</subject><subject> Social Sciences&amp;Humanities</subject></subj-group></article-categories><title-group><article-title>
 
 
  The Cause of the Gleissberg Cycle: A Working Hypothesis
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sebastián</surname><given-names>Martín Ruiz</given-names></name><xref ref-type="aff" rid="aff1"><sub>1</sub></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><label>1</label><addr-line>Avda. De Regla, Chipiona, Spain</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>smruiz@telefonica.net</email></corresp></author-notes><pub-date pub-type="epub"><day>31</day><month>12</month><year>2015</year></pub-date><volume>02</volume><issue>12</issue><fpage>1</fpage><lpage>5</lpage><history><date date-type="received"><day>2</day>	<month>December</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>16</month>	<year>December</year>	</date><date date-type="accepted"><day>22</day>	<month>December</month>	<year>2015</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
   
   Gleissberg cycle is a recurring climatic period of 80 years duration. It is usually attributed to the influence of the Sun. In this article, we present a new hypothesis for the possible cause related to the magnetic field of Jupiter. 
  
 
</p></abstract><kwd-group><kwd>Gleissberg Cycle</kwd><kwd> Maunder Minimum</kwd><kwd> Cosmic Rays</kwd><kwd> Jupiter’s Magnetic Field</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The Gleissberg cycle (<xref ref-type="fig" rid="fig1">Figure 1</xref>) is a 80-year climatic cycle which causes climatic cycle [<xref ref-type="bibr" rid="scirp.69006-ref1">1</xref>] the famous Maunder Minimum (<xref ref-type="fig" rid="fig2">Figure 2</xref>) that apparently originates the Little Ice Age. The intensity variation of this cycle is more or less the same order as the solar cycles of 11 years but with the difference that occurs in a longer period of time sufficient to make significant climatic changes.</p><p>The Gleissberg cycle may be the main cause of these variations in global temperatures.</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> The smooth curve of temperatures between 1880 and 2010 has sinusoidal shape and its maximum is about 1900 and 1980 therefore it has a period of approximately 80 years</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/69006x6.png"/></fig><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> The Maunder Minimum occurred between 1645 and 1715</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/69006x7.png"/></fig><p>The Gleissberg cycle is usually attributed to a solar activity cycle. But we think it may have another possible, cause.</p></sec><sec id="s2"><title>2. Cosmic Rays</title><p>Anyway we should consider the recent research on the influence of the cosmic rays on the weather.</p><p>The scientist Henrik Svensmark [<xref ref-type="bibr" rid="scirp.69006-ref2">2</xref>] [<xref ref-type="bibr" rid="scirp.69006-ref3">3</xref>] , director of the Research Center of the Sun-Climate Relationship was surprised “by the speed and efficiency of how the electrons work to create the main blocks for the cloud condensation nuclei”.</p><p>The results of this experiment supports the empirical theory proposed a decade ago (made by scientists Henrik Svensmark and Eigil Friis-Christensen), that cosmic rays influences the Earth’s climate through cloud formation (<xref ref-type="fig" rid="fig3">Figure 3</xref>). The original theory showing the correlation between the change in the intensity of cosmic rays entering our atmosphere and the amount of clouds located at a low altitude. Cloud cover increases when the cosmic ray intensity increases and decreases when the intensity declines.</p><p>It is known that low-altitude clouds have a cooling effect on the Earth’s surface so that variations in cloud</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Cosmic rays influence the creation of clouds</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/69006x8.png"/></fig><p>covering caused by cosmic rays could, in turn, change the temperature of the surface.</p><p>The existence of this connection between cosmic rays and the Earth’s climate could explain past and present variations of our climate.</p></sec><sec id="s3"><title>3. The Possible Effect of Jupiter</title><p>We should wonder what can produce a 80-year cycle in cosmic radiation reaching the Earth. To vary the cosmic radiation striking the Earth in a 80-year cycle, we would need to have a magnetic shield that rotates against the background of fixed stars every 80 years or so. Well, we have it. It is the planet Jupiter [<xref ref-type="bibr" rid="scirp.69006-ref4">4</xref>] - [<xref ref-type="bibr" rid="scirp.69006-ref6">6</xref>] , although its visible radiation from the Earth is small, we all know that it has a magnetic field (<xref ref-type="fig" rid="fig4">Figure 4</xref>) as seen from Earth is greater than the full Moon. This could be deflecting the cosmic radiation coming from outside the solar system. And the position of Jupiter, seen from Earth, as regards to the fixed stars varies precisely in a period of approximately 80 years [<xref ref-type="bibr" rid="scirp.69006-ref7">7</xref>] . This is because the orbital period of Jupiter is 11.86 years and 11.86 &#215; 7 = 83.02. Every 83</p><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Jupiter’s magnetic field is much larger than the planet already giant</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/69006x9.png"/></fig><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Intensity of cosmic radiation (solid line) from 1953 to date detected in the monitor climax, United States, along with the sunspot cycle (dotted line) for the same period</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/69006x10.png"/></fig><p>years, Jupiter and the Earth are in the same relative position in the Solar System and this way Jupiter is seen against the same background of stars.</p><p>According to this hypothesis it would be interesting to study the frequency of radiation coming from outside the solar system like the solar [<xref ref-type="bibr" rid="scirp.69006-ref8">8</xref>] - [<xref ref-type="bibr" rid="scirp.69006-ref11">11</xref>] radiation that correlates [<xref ref-type="bibr" rid="scirp.69006-ref12">12</xref>] with sunspots (<xref ref-type="fig" rid="fig5">Figure 5</xref>).</p></sec><sec id="s4"><title>4. Conclusion</title><p>In conclusion, we think that the influence of Jupiter’s magnetic field on cosmic rays reaching the Earth and its relationship to Earth’s climate should be investigated.</p></sec><sec id="s5"><title>Cite this paper</title><p>Sebasti&#225;n Mart&#237;n Ruiz, (2015) The Cause of the Gleissberg Cycle: A Working Hypothesis. Open Access Library Journal,02,1-5. doi: 10.4236/oalib.1102203</p></sec></body><back><ref-list><title>References</title><ref id="scirp.69006-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">(2011) Historia de los cambios climáticos. Comellas Garcia Llera, Jose Luis (RIALP).</mixed-citation></ref><ref id="scirp.69006-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">(2003) The Chilling Stars: A New Theory of Climate Change by Henrik Svensmark and Nigel Calder.</mixed-citation></ref><ref id="scirp.69006-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">(2004) The Chilling Stars: A Cosmic View of Climate Change by Henrik Svensmark and Nigel Calder.</mixed-citation></ref><ref id="scirp.69006-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Rogers, J.H. (1995) The Giant Planet Jupiter. Cambridge University Press, Cambridge.</mixed-citation></ref><ref id="scirp.69006-ref5"><label>5</label><mixed-citation publication-type="other" xlink:type="simple">Bagenal, F., Dowling, T.E., McKinnon, W.B., Jewitt, D., Murray, C., Bell, J., Lorentz, R. and Nimmo, F. (2004) Jupiter: The Planet, Satellites and Magnetosphere. Cambridge University Press, Cambridge.</mixed-citation></ref><ref id="scirp.69006-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Sagan, C. (1961) El Sistema Solar. Blume-Hermann, Madrid.</mixed-citation></ref><ref id="scirp.69006-ref7"><label>7</label><mixed-citation publication-type="other" xlink:type="simple">Fernando Beltrán Postigo: Personal Communication: Investigation of Orbital Period of Jupiter.https://www.youtube.com/user/fernandobeltranp</mixed-citation></ref><ref id="scirp.69006-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">de Madrid, A.A. (1998) Manual de Astronomía Práctica. Agrupaci&amp;#243;n Astron&amp;#243;mica de Madrid.</mixed-citation></ref><ref id="scirp.69006-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Astronomía. COMELLAS, JOSE LUIS. Sevilla. Rialp 1987.</mixed-citation></ref><ref id="scirp.69006-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">Estrellas. HERRMANN, J. Barcelona Blume 1986.</mixed-citation></ref><ref id="scirp.69006-ref11"><label>11</label><mixed-citation publication-type="other" xlink:type="simple">(1994) El Sol: Nuestro astro. II Curso de Introducci&amp;#243;n a la Astronomía. HIDALGO RODRIGUEZ, INéS (CICCA-IAC).</mixed-citation></ref><ref id="scirp.69006-ref12"><label>12</label><mixed-citation publication-type="other" xlink:type="simple">http://bibliotecadigital.ilce.edu.mx/sites/ciencia/volumen3/ciencia3/108/htm/sec_10.htm</mixed-citation></ref></ref-list></back></article>